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Marine heatwaves are human made

Marine heatwaves have increased significantly due to global warming, with major events becoming more frequent and prolonged. The probability of such events has risen massively, posing a serious threat to marine ecosystems and their ability to recover.

SourceUniversity of Bern·JournalScience·DateSep 25, 2020

Reconstructing global climate through Earth's history

Researchers have developed a framework to reconcile discrepancies in ancient sea surface temperature estimates and climate model results. By accounting for location-biased paleoclimate data, scientists can better reconstruct global climate conditions in the past and improve predictions of future climate scenarios.

SourceSyracuse University·JournalGeophysical Research Letters·DateAug 13, 2020

Climate predictions several years into the future?

A study by GEOMAR Helmholtz Centre for Ocean Research Kiel predicts North Atlantic surface temperature variations several years into the future using wind field analysis. The researchers suggest a mechanism where winds cause changes in ocean circulation, resulting in anomalous heat accumulation and warming of the eastern North Atlantic.

SourceHelmholtz Centre for Ocean Research Kiel (GEOMAR)·JournalGeophysical Research Letters·DateJul 22, 2020

Going against the trend

Researchers discovered that sea-ice changes are the most probable cause for the cooling of surface waters in the Southern Ocean. Simulations show that stronger winds propelled sea ice into the open ocean, enhancing freshwater transport and creating a stratified seawater layer with reduced heat exchange.

SourceETH Zurich·JournalAGU Advances·DateMay 6, 2020

Climate change and precipitation in Mediterranean climates

A study reveals that Mediterranean-like climates are experiencing variable responses to climate warming, with some regions drying faster than global-mean warming. The differences result from distinct regional changes in atmospheric circulation driven by separate fast and slow sea-surface temperature responses to greenhouse gases.

SourceProceedings of the National Academy of Sciences·JournalProceedings of the National Academy of Sciences·DateFeb 17, 2020

Acid-loving microbe can improve understanding of past climate

Researchers from Dartmouth College used an acid-loving microbe to improve the accuracy of past climate records by studying its response to food and energy availability. The findings suggest that factors other than temperature can influence the membranes of single-celled archaea, adding complexity to paleoclimate studies.

SourceDartmouth College·JournalEnvironmental Microbiology·DateFeb 10, 2020

The heat is on

An international team of scientists analyzed 3 million species records from 200 ecological communities worldwide to reveal the impact of ocean warming on fish communities. The study found that subtle changes in species movement in response to rising temperatures made a significant impact on the global picture.

SourceUniversity of California - Santa Barbara·JournalNature Climate Change·DateNov 25, 2019

Correcting historic sea surface temperature measurements

Researchers from Harvard University and the UK's National Oceanography Centre corrected historic sea surface temperature measurements, identifying two new key causes of warming discrepancies in the North Pacific and North Atlantic. The study suggests that changes in Japanese records, particularly truncation of data, contributed to the ...

NASA study verifies global warming trends

A NASA study has verified recent global warming figures, showing high consistency between satellite-based AIRS data and station-based GISTEMP analysis over the past 15 years. The findings also suggest that surface-based data may be underestimating temperature changes in the Arctic, indicating faster warming at the poles.

SourceIOP Publishing·JournalEnvironmental Research Letters·DateApr 16, 2019

Cold reminders of Earth's last great cold snap revealed in the deep Pacific

A new study has found evidence of a centuries-long cold snap in the deep Pacific, with ongoing cooling indicating the ocean is still adjusting to surface cooling during the Little Ice Age. The research suggests that the heat loss in the deep Pacific since 1750 offsets nearly a quarter of global heat gain in the upper ocean.